Stratigraphic Patterns in Carbonate Source-Rock Distribution: Second-Order to Fourth-Order Control and Sediment Flux

2005 ◽  
pp. 191-223 ◽  
Author(s):  
F.S.P. van BUCHEM ◽  
A.Y. HUC ◽  
BERNARD PRADIER ◽  
MARCO M. STEFANI
Keyword(s):  
Source Rock ◽  
Fourth Order ◽  
Second Order ◽  
Sediment Flux ◽  
Carbonate Source Rock ◽  
Carbonate Source

First Successful Proppant Fracture for Unconventional Carbonate Source Rock in Saudi Arabia

2014 ◽  
Author(s):  
Nayef Ibrahim Al-Mulhim ◽  
Ali Hussein Al-Saihati ◽  
Ahmed M. Hakami ◽  
Moataz Al-Harbi ◽  
Khalid Saeed Asiri
Keyword(s):  
Saudi Arabia ◽  
Source Rock ◽  
Carbonate Source Rock ◽  
Carbonate Source

scholarly journals Method for identifying effective carbonate source rocks: a case study from Middle–Upper Ordovician in Tarim Basin, China

2020 ◽  
Vol 17 (6) ◽  
pp. 1491-1511
Author(s):  
Jun-Qing Chen ◽  
Xiong-Qi Pang ◽  
Song Wu ◽  
Zhuo-Heng Chen ◽  
Mei-Ling Hu ◽  
...  
Keyword(s):  
Crude Oil ◽  
Source Rock ◽  
Tarim Basin ◽  
Fluid Pressure ◽  
Source Rocks ◽  
Hydrocarbon Generation ◽  
Upper Ordovician ◽  
Carbonate Source Rock ◽  
Carbonate Source ◽  
Effective Source

AbstractHydrocarbon expulsion occurs only when pore fluid pressure due to hydrocarbon generation in source rock exceeds the force against migration in the adjacent carrier beds. Taking the Middle–Upper Ordovician carbonate source rock of Tarim Basin in China as an example, this paper proposes a method that identifies effective carbonate source rock based on the principles of mass balance. Data from the Well YW2 indicate that the Middle Ordovician Yijianfang Formation contains effective carbonate source rocks with low present-day TOC. Geological and geochemical analysis suggests that the hydrocarbons in the carbonate interval are likely self-generated and retained. Regular steranes from GC–MS analysis of oil extracts in this interval display similar features to those of the crude oil samples in Tabei area, indicating that the crude oil probably was migrated from the effective source rocks. By applying to other wells in the basin, the identified effective carbonate source rocks and non-source rock carbonates can be effectively identified and consistent with the actual exploration results, validating the method. Considering the contribution from the identified effective source rocks with low present-day TOC (TOCpd) is considered, the long-standing puzzle between the proved 3P oil reserves and estimated resources in the basin can be reasonably explained.

Dysaerobic carbonate source rock - Lower Cretaceous of provence South-East France

1996 ◽  
Author(s):  
L. Machhour ◽  
J. P. Masse ◽  
B. Lambert ◽  
Ph. Lapointe ◽  
J. -L. Oudin
Keyword(s):  
Source Rock ◽  
Lower Cretaceous ◽  
Carbonate Source Rock ◽  
Carbonate Source
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